湖北农业科学 ›› 2026, Vol. 65 ›› Issue (8): 65-73.doi: 10.14088/j.cnki.issn0439-8114.2026.08.010

• 资源·环境 • 上一篇    下一篇

昌吉回族自治州灌耕土的发生特性及其在中国土壤系统分类中的归属

王帅帅, 武红旗, 范燕敏, 郭佳, 毕延安, 商舒皓   

  1. 新疆农业大学资源与环境学院/新疆土壤与植物生态过程重点实验室,乌鲁木齐 830052
  • 收稿日期:2026-05-19 发布日期:2026-09-02
  • 通讯作者: 范燕敏(1975-),女,副教授,博士,主要从事土壤质量检测与评价研究,(电子信箱)ymfantt@126.com。
  • 作者简介:王帅帅(1999-),男,河南尉氏人,在读硕士研究生,研究方向为土壤学,(电子信箱)320223559@xjau.edu.cn
  • 基金资助:
    西北盐渍土区土壤改良与产能提升技术模式集成和示范项目(2023YFD1901503)

Genesis characteristics of irrigated cultivated soils in Changji Hui Autonomous Prefecture and taxonomic positions in Chinese Soil Taxonomy

WANG Shuai-shuai, WU Hong-qi, FAN Yan-min, GUO Jia, BI Yan-an, SHANG Shu-hao   

  1. College of Resources and Environment, Xinjiang Agricultural University/Xinjiang Key Laboratory of Soil and Plant Ecological Process, Urumqi 830052, China
  • Received:2026-05-19 Online:2026-09-02

摘要: 为区域耕地资源精准规划、耕地质量提升及农业可持续发展提供坚实的土壤分类学依据,从昌吉回族自治州选取15个代表性灌耕土剖面,通过对剖面形态特征观测和理化性质分析,确定其诊断层与诊断特性;依据《中国土壤系统分类检索》(第三版)进行分类检索,参照土族和土系划分标准构建基层分类单元,并与发生分类结果进行参比分析。结果表明,研究区灌耕土剖面层次分化清晰,发生分类中可划分为灌淤土和灌漠土2个土类;在系统分类中,15个剖面共归属于2个土纲2个亚纲2个土类3个亚类8个土族15个土系。由所有剖面在高级与基层分类单元上发生分类与系统分类的对应及参比结果可知,昌吉回族自治州灌耕土的发生分类与系统分类并不是一一对应关系,其中灌漠土剖面经长期人为耕作干预已形成具有明显熟化特征的表层及稳定发育的诊断表下层,但该类土壤不满足现行《中国土壤系统分类检索》(第三版)中对应人为土的检索条件,仅能被归为雏形土纲,无法精准反映人为耕作活动对其成土过程和土壤属性的主导影响,导致分类结果与土壤实际发育特征不匹配。基于此,建议在中国土壤系统分类中增设“灌漠表层”诊断表层及“灌漠旱耕人为土”土类。

关键词: 灌耕土, 发生特性, 归属, 中国土壤系统分类, 昌吉回族自治州

Abstract: To provide a solid pedotaxonomic basis for the precise planning of regional cultivated land resources, improvement of cultivated land quality and sustainable agricultural development, fifteen representative profiles of irrigated cultivated soils were selected from Changji Hui Autonomous Prefecture. Diagnostic horizons and diagnostic characteristics were identified through field observation of profile morphological features and laboratory analysis of soil physicochemical properties. Taxonomic classification was conducted in accordance with the Keys to Chinese Soil Taxonomy (3rd Edition). Basic taxonomic units were established following the criteria for soil family and soil series classification, and a comparative analysis was further carried out between the results of genetic soil classification and Chinese Soil Taxonomy. The results showed that there was obvious horizon differentiation in all profiles of irrigated cultivated soils in the study area, which were classified into two great groups (irrigated silting soils and irrigated desert soils) under genetic soil classification. Under Chinese Soil Taxonomy, the 15 soil profiles belong to 2 soil orders, 2 suborders, 2 great groups, 3 subgroups, 8 soil families and 15 soil series. The comparison between genesis classification and Chinese Soil Taxonomy at both higher and basic taxonomic levels indicated that there was no one-to-one correspondence between the two classification systems for irrigated cultivated soils in Changji Hui Autonomous Prefecture. Long-term anthropogenic cultivation had formed surface horizons with obvious anthropic maturing features and well-developed subsurface diagnostic horizons in the profiles of irrigated desert soils. However, such soils failed to meet the retrieval criteria for Anthrosols specified in the current Keys to Chinese Soil Taxonomy (3rd Edition), and were consequently classified into the order Cambisols. This classification could not accurately reflect the dominant impacts of anthropogenic cultivation on soil-forming processes and soil properties, leading to inconsistencies between taxonomic results and actual soil development characteristics. Accordingly, it was proposed to establish a new diagnostic surface horizon named irrigated desert epipedon and a new great group irrigated desert orthic anthrosols in the Chinese Soil Taxonomy.

Key words: irrigated cultivated soil, genesis characteristics, taxonomic position, Chinese Soil Taxonomy, Changji Hui Autonomous Prefecture

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